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Table 1

Selected parameters from the best-fit PoWRHD models of the six targets in this study.

Parameter(a) WR 1 WR 6 WR 7 WR 18 WR 37 WR 58
R* (R) 1.076 ± 0.04 0.7300.04+0.06Mathematical equation: $0.730_{-0.04}^{+0.06}$ 0.564 ± 0.08 1.2070.06+0.08Mathematical equation: $1.207_{-0.06}^{+0.08}$ 0.973 ± 0.08 0.5100.08+0.09Mathematical equation: $0.510_{-0.08}^{+0.09}$
Rcrit (R) 1.101 0.528 0.584 1.234 1.001 0.475
Rτ=2/3 (R) 3.421 1.987 2.128 5.377 3.880 2.034
T*(b) (kK) 140 ± 2.4 143 ± 1.6 145 ± 2.7 140 ± 1.6 143 ± 0.8 144 ± 2.6
Teff (Rcrit) (kK) 138.4 141.0 142.5 138.4 141.0 141.4
Tτ = 2/3} (kK) 78.5 86.7 74.6 66.3 71.6 72.1
log10(L* (L)) 5.6 ± 0.08 5.30.08+0.12Mathematical equation: $5.3_{-0.08}^{+0.12}$ 5.1 ± 0.16 5.70.12+0.16Mathematical equation: $5.7_{-0.12}^{+0.16}$ 5.6 ± 0.16 5.00.16+0.18Mathematical equation: $5.0_{-0.16}^{+0.18}$
M* (M) 19.6 ± 1.25 10.3 ± 0.27 6.0 ± 0.56 22.3 ± 3.39 14.5 ± 1.28 4.9 ± 0.84
log10 ( (M yr−1)) −4.9 ± 0.06 5.10.06+0.09Mathematical equation: $-5.1_{-0.06}^{+0.09}$ −5.2 ± 0.12 4.70.09+0.12Mathematical equation: $-4.7_{-0.09}^{+0.12}$ −4.8 ± 0.12 5.30.12+0.14Mathematical equation: $-5.3_{-0.12}^{+0.14}$
log10 (t (M yr−1)) −3.9 ± 0.12 4.00.12+0.18Mathematical equation: $-4.0_{-0.12}^{+0.18}$ −4.0 ± 0.24 4.10.18+0.24Mathematical equation: $-4.1_{-0.18}^{+0.24}$ −4.0 ± 0.24 4.00.24+0.28Mathematical equation: $-4.0_{-0.24}^{+0.28}$
υ (km s−1) 2023 ± 288 1759 ± 179 1328 ± 175 1603 ± 216 1788 ± 117 1225 ± 300
D(c)Mathematical equation: $D_\infty^{(c)}$ 70 50 20 15 20 20

Notes. (a)All models have a microturbulent velocity of υmic = 30 km s−1. (b)The effective temperature at the inner boundary R*, set at τRoss,cont = 20. (c)We adopted a depth-dependent clumping law (Hillier et al. 2003) where we used 100 km s−1 as the onset velocity υcl (250 km s−1 for WR 58) and where D represents the clumping when υ >> υcl.

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